Geophysical Research Abstracts, Vol. 7, 01904, 2005 SRef-ID: 1607-7962/gra/EGU05-A-01904
© European Geosciences Union 2005
Distribution and sources of organic carbon in a
mangrove-seagrass ecosystem (Gazi Bay, Kenya)
S. Bouillon (1), F. Dehairs (1), G. Abril (2), A.V. Borges (3)
(1) Dept. of Analytical and Environmental Chemistry, Vrije Universiteit Brussel, (2) Environnements et Paléoenvironnements Océaniques, Université Bordeaux 1, (3) Unité d’Océanographie Chimique, University of Liège. (steven.bouillon@vub.ac.be / Fax : +32 2 6293274)
The concentrations and stable isotope composition of different organic carbon pools was studied in Gazi Bay (Kenya 4.4˚S 39.5˚E), in July 2003. Gazi Bay is a shallow tropical coastal ecosystem, with extensive mangrove forests intersected by 2 main tidal creeks (Kidogoweni and Kinondo), and a shallow bay largely covered by dense Thalassodendron ciliatum seagrass beds. The distribution of organic carbon along the salinity gradient of the tidal creeks indicated significant internal inputs of organic carbon, with a δ13C signature consistent with that of the dominant vegetation, i.e. mangroves. Low water column Chl a values and high POC/Chl a ratios are indica-tive of the predominance of macrophyte material or highly degraded organic matter in the water column. At the boundary of the mangrove-seagrass interface, however, coinciding with a salinity of ∼30, the carbon isotope composition of POC changes drastically, from about -27 %¸ to values as high as -14 %¸, indicative of a geograph-ically sharp change in the relative contribution of mangrove and seagrass-derived or-ganic carbon. The sedimentary record, however, does indicate that mangrove carbon is exported from the system boundaries and trapped in the seagrass beds adjacent to the mangrove forest where it contributes to benthic mineralization. On the other hand, seagrass material is similary imported into the mangrove areas, but the contribution of seagrass material in mangrove sediments appears to be limited, overall. The high spatial variability in the sources of the aquatic organic carbon pool is also mirrored in the distribution of pCO2, %O2, δ13C signature of DIC and δ18O signature of dissolved O2, which indicate a distinct gradient from a highly heterotrophic system (mangrove creeks) to a net autotrophic region (seagrass beds). Overall, the data indicate that
ex-port of mangrove-derived organic carbon is limited to a geographically limited area close to the forest boundary, and unlikely to reach the coastal shelf area.
